Scientist Andrew Fountain samples a patch of wet, salty soil in Taylor Valley. Researchers discovered that the salty soils in the McMurdo Dry Valleys can draw moisture out of the air to create wet patches of ground.

Drawing it out

Scientists link salty soils to wet patches in the McMurdo Dry Valleys

By Peter Rejcek, Antarctic Sun Editor

Posted March 16, 2012

Permafrost geologist Joseph Levy calls the salty tale of water formation on the floor of the McMurdo Dry Valleys the story of how Antarctica got its spots.

He and colleagues noticed patches of wet and damp soil — but it was well below freezing that day. Scratching their heads — and being curious, as scientists are — they collected some of the dirt and analyzed the samples.

The study, which was supported by the National Science Foundation, was recently published online in the journal Geophysical Research Letters. It will also appear in a forthcoming printed edition.

Levy said the process was first predicted more than 30 years ago by scientist Alexander Wilson at Victoria University of Wellington, who was investigating the lakes in the Dry Valleys, particularly a super briny body of water called Don Juan Pond. Wilson suggested salty soils on mountain peaks pulled moisture out of the air, the brine percolating down the valley walls and into the lakes.

“It looks like the process happens everywhere in the Dry Valleys that you have these wet patches,” Levy said. “It’s how Antarctica got its spots. It’s pretty common.”

A simple experiment confirmed the hypothesis. Levy put the salty soils into one jar and water into a second jar, then sealed both into a plastic container. The soil was soaking wet after a couple of days.

“The same thing happens in the Dry Valleys,” he said, adding that the process only requires high humidity to act as a catalyst. Once a brine forms by sucking water vapor out of the air, the brine will keep collecting water vapor until it equalizes with the atmosphere.

And where there is water, there is life.

“We know those wet patches are little oases in the cold desert,” Levy said. The carbon content is about 30 times higher than in adjacent areas, providing plenty of fuel for microorganisms inhabiting the soils.

The find has implications for scientists interested in understanding how far out places like Mars might support life.

In fact, the Mars analog to the Dry Valleys might explain the appearance of dark stripes found along the slopes of Martian mountains during the spring and summer. Levy said the pattern is similar to the one displayed by liquid brines moving over the permafrost surface of the Taylor Valley.

“Every year, Mars looks more like Antarctica to me and Antarctica looks more like Mars,” Levy said.

NSF-funded research in this article: Joseph Levy, Oregon State University, Award No. 0851965.Other authors on the study include Andrew Fountain, Portland State University, and Kathy Welch and W. Berry Lyons, The Ohio State University.